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Early Paleozoic tectonism within the East Antarctic craton: The final suture between east and west Gondwana?

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Boger, Steven D.
Wilson, Colin J
Fanning, Christopher

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Geological Society of America Inc

Abstract

New U-Pb SHRIMP ages from East Antarctica point to the existence of a laterally continuous orogenic belt that bisects the East Antarctic craton. This orogenic belt juxtaposes Archean crust to the south and east against Neoproterozoic metamorphic rocks to

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Geology

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